The orthopyroxene series runs between enstatite, Mg2Si2O6, and ferrosilite, Fe2+2Si2O6, by the same iron–magnesium substitution that governs olivine; augite, the common clinopyroxene, carries a formula written with variable cations because its composition genuinely varies.
Evidence support: Supported by the cited evidence one source
Evidence: Commission on New Minerals, Nomenclature and Classification, International Mineralogical Association 2026 Primary authority
